
浏览全部资源
扫码关注微信
1. 西北农林科技大学 水土保持研究所, 陕西 杨凌,712100
2. 中国科学院 教育部 水土保持与生态环境研究中心, 陕西 杨凌,712100
Published:2024
移动端阅览
Zhao Ting, Wu Binglong, Zheng Fenli, et al. Conversion of Low-resolution Slope Gradient Based on Histogram Matching at Rolling Hilly Area of Northeast China[J]. Bulletin of Soiland Water Conservation, 2024, 44(6): 149-158.
Zhao Ting, Wu Binglong, Zheng Fenli, et al. Conversion of Low-resolution Slope Gradient Based on Histogram Matching at Rolling Hilly Area of Northeast China[J]. Bulletin of Soiland Water Conservation, 2024, 44(6): 149-158. DOI: 10.13961/j.cnki.stbctb.2024.06.016.
[目的] 为了克服目前可免费下载的30 m分辨率DEM在提取东北漫川漫岗地貌区耕地坡度时存在的坡度变缓问题,获取精确坡度数据,为东北漫川漫岗地貌类型区土壤侵蚀定量评价提供重要数据支持。[方法] 基于无人机航测影像生成5 cm分辨率DEM并对其重采样获得1,5和12.5 m分辨率的DEM,结合免费下载的30 m分辨率DEM,确定研究区DEM提取坡度的最佳分辨率;基于直方图匹配算法,分坡度段拟合了30 m与最佳分辨率DEM之间的坡度转换模型。[结果] ①5组DEM分辨率提取的坡度信息表明,1和5 m与5 cm分辨率DEM提取的坡度分布频率具有较强的相似性,且5 m分辨率DEM与1∶10 000比例尺地形图的分辨率相对应。据此确定5 m分辨率为构建坡度转换模型的最佳分辨率。②基于直方图匹配算法分坡度段构建了30与5 m分辨率DEM提取坡度的一元一次线性模型和一元二次非线性模型;且当地面坡度小于7°时宜选取线性坡度转换模型,而当地面坡度大于7°时宜选取非线性坡度转换模型。③经线性和非线性坡度转换模型优化后,30 m坡度分布频率与5 m分辨率的坡度分布频率基本相似,且协方差、相关系数均大幅度提高。这说明30 m分辨率DEM提取的坡度信息经模型转换后能够真实反映地面起伏特征,且非线性坡度转换模型优化效果更佳。[结论] 5 m分辨率为研究区DEM提取坡度的最佳分辨率。构建的低—高分辨率的坡度转换模型中,非线性坡度转换模型较线性坡度转换模型的优化效果更好。
[Objective] Slope gradient data was accurately obtained to address the limitation of slope gradient underestimation using the freely downloaded 30 m resolution digital elevation model (DEM) for farmland in Northeast China
in order to provide important data support for quantitatively evaluating soil erosion in the rolling hilly regions. [Methods] A 5 cm resolution DEM was generated from drone survey images and resampled to obtain 1
5
and 12.5 m DEM resolutions. Combined with the 30 m DEM resolution
the optimal DEM resolution for slope gradient extraction in the study area was identified. Additionally
the histogram matching method was used to establish a slope gradient conversion model between the 30 m DEM resolution and the optimal DEM resolution for each slope gradient category. [Results] ① The slope gradient distributions derived from the five DEM resolutions indicated that the 1 m and 5 m DEM resolutions exhibited a strong similarity to the slope gradient distribution of the 5 cm DEM. Given that the 5 m DEM resolution corresponds to a 1∶10
000 scale topographic map
the 5 m DEM resolution was optimal for constructing the slope gradient conversion model. ② Using the histogram matching method
a univariate linear model and a univariate quadratic non-linear model were developed for slope gradient conversion between the 30 m and 5 m DEM resolutions across different slope gradient segments. The linear conversion model was suitable for slopes less than 7°
while the non-linear model was more appropriate for slopes greater than 7°. ③ After applying both linear and non-linear conversion models
the frequency distribution of slope gradients extracted from the 30 m DEM resolution closely matched that of the 5 m DEM resolution
significantly improving covariance and correlation coefficients. This reflected that the slope gradients after conversion from the 30 m DEM resolution can accurately represent ground undulation; additionally
the optimization results from the non-linear conversion model were superior to those from the linear conversion model. [Conclusion] The 5 m DEM resolution is the optimal resolution for extracting slope data in the study area. The developed conversion model for low-to-high resolution slope gradients showed that the non-linear slope conversion model has a better optimization effect than the linear slope conversion model.
Lu Shaojuan, Liu Baoyuan, Hu Yaxian, et al. Soil erosion topographic factor (
LS
): Accuracy calculated from different data sources [J]. Catena, 2020,187:104334.
杨维鸽,郑粉莉,王占礼,等.地形对黑土区典型坡面侵蚀—沉积空间分布特征的影响[J].土壤学报,2016,53(3):572-581. Yang Weige, Zheng Fenli, Wang Zhanli, et al. Effects of topography on spatial distribution of soil erosion and deposition on hillslope in the typical of black soil region [J]. Acta Pedologica Sinica, 2016,53(3):572-581.
张晓平, 梁爱珍, 申艳, 等.东北黑土水土流失特点[J].地理科学,2006,26(6):687-692. Zhang Xiaoping, Liang Aizhen, Shen Yan, et al. Erosion characteristics of black soils in Northeast China [J]. Scientia Geographica Sinica, 2006,26(6):687-692.
An Juan, Zheng Fenli, Wang Bin. Using
137
Cs technique to investigate the spatial distribution of erosion and deposition regimes for a small catchment in the black soil region, Northeast China [J]. Catena, 2014,123:243-251.
蔡清华,杨勤科.SRTM与地形图生成DEM的地形表达能力对比[J].水土保持通报,2009,29(3):183-187. Cai Qinghua,Yang Qinke. Comparison of terrain representation of SRTM and topographic derived DEMs [J]. Bulletin of Soil and Water Conservation, 2009,29(3):183-187.
土祥,王春梅,庞国伟,等.黄土丘陵沟壑区坡度尺度效应空间分异分析[J].山地学报,2018,36(6):964-972. Tu Xiang, Wang Chunmei, Pang Guowei, et al. On the spatial differentiation of scale effect of slopes in loess hill and gully region, China [J]. Mountain Research, 2018,36(6):964-972.
Grohmann C H. Effects of spatial resolution on slope and aspect derivation for regional-scale analysis [J]. Computers & Geosciences, 2015,77:111-117.
罗为东,甘淑,袁希平,等. 基于UAV高分辨率DEM的复杂微地貌形态特征分析:以恐龙谷南缘山区为例[J]. 中国水土保持科学, 2022, 20(5): 109-117. Luo Weidong, Gan Shu, Yuan Xiping, et al. Morphological characterization of complex micro-landscapes based on UAV high-resolution DEM: Take the mountainous area on the southern rim of Dinosaur Valley as an example [J]. Science of Soil and Water Conservation, 2022,20(5): 109-117.
Altunel A O, Okolie C J, Kurtipek A. Capturing the level of progress in vertical accuracy achieved by ASTER GDEMsince the beginning: Turkish and Nigerian examples [J]. Geocarto International, 2022,37(26):12073-12095.
Munoth P, Goyal R. Effects of DEM source,spatial resolution and drainage area threshold values on hydrological modeling [J]. Water Resources Management, 2019,33(9):3303-3319.
汤国安,杨勤科,张勇,等.不同比例尺DEM提取地面坡度的精度研究:以在黄土丘陵沟壑区的试验为例[J].水土保持通报,2001,21(1):53-56. Tang Guoan, Yang Qinke, Zhang Yong, et al. Research on accuracy of slope derivedfrom DEMs of different map scales [J]. Bulletin of Soil and Water Conservation, 2001,21(1):53-56.
刘飞,范建容,崔兆岩,等.基于DEM分形特征的坡度尺度变换模型[J].山地学报,2019,37(1):129-136. Liu Fei, Fan Jianrong, Cui Zhaoyan, et al. A model of re-scaling slope based on DEM fractal feature [J]. Mountain Research, 2019,37(1):129-136.
Zhang Xiaoyang, Drake N A, Wainwright J, et al. Comparison of slope estimates from low resolution DEMs: Scaling issues and a fractal method for their solution [J]. Earth Surface Processes and Landforms, 1999,24(9):763-779.
Yang Qinke, Jupp D, Li Rui, et al. Re-scaling lower resolution slope by histogram matching [M]//Lecture Notes in Geoinformation and Cartography. Berlin & Heidelberg, Germany: Springer, 2008.
Jou F D, Fan K C, Chang Yanglang. Efficient matching of large-size histograms[J]. Pattern Recognition Letters, 2004,25(3):277-286.
Wang Chunmei, Shan Linxin, Liu Xin, et al. Impacts of horizontal resolution and downscaling on the USLE
LS
factor for different terrains [J]. International Soil and Water Conservation Research, 2020,8(4):363-372.
汤国安,张友顺,刘咏梅.遥感数字图像处理[M]. 北京:科学出版社,2004. Tang Guoan, Zhang Youshun, Liu Yongmei. Remote sensing digital image processing [M]. Beijing: China Science Press, 2004.
张荞,张艳梅,蒙印.基于直方图匹配的多源遥感影像匀色研究[J].地理空间信息,2020,18(12):54-57. Zhang Qiao, Zhang Yanmei, Meng Yin. Researchon color uniforming for multi-source remote sensing images based on histogram matching method [J]. Geospatial Information, 2020,18(12):54-57.
王琦,杨勤科,任宗萍.中尺度流域NDVI尺度转换研究[J].水土保持通报,2010,30(3):96-99. Wang Qi, Yang Qinke, Ren Zongping. Scaling of ETM-NDVI for medium watershed area [J]. Bulletin of Soil and Water Conservation, 2010,30(3):96-99.
师动,朱奇峰,杨勤科,等.DEM分辨率对坡度算法选择影响的分析[J].山地学报,2020,38(6):935-944. Shi Dong, Zhu Qifeng, Yang Qinke, et al. DEM resolution influence on slope algorithm selection [J]. MountainResearch, 2020,38(6):935-944.
杨颖楠,李子夫,刘梦云,等.基于不同分辨率DEM的永寿县地形信息差异分析[J].水土保持研究,2018,25(6):131-136. Yang Yingnan, Li Zifu, Liu Mengyun, et al. Analysis of topographic differences of Yongshou County based on different resolutions of DEM [J]. Research of Soil and Water Conservation, 2018,25(6):131-136.
陈楠.DEM分辨率与平均坡度的关系分析[J].地球信息科学学报,2014,16(4):524-530. Chen Nan. Relationship between DEM resolution and average slope derived from DEM [J]. Journal of Geo-Information Science, 2014,16(4):524-530.
Chen Xue, Chen Guokun, Feng Junxin, et al. Slope scaling effect and slope-conversion-atlas for typical water erosion regions in China [J]. Sustainability, 2023,15(4):3789.
张永红,黄付强,程华,等.两种分辨率DEM在不同空间尺度下的差异:以黄土高原丘陵区为例[J].西部林业科学,2020,49(4):54-59,67. Zhang Yonghong, Huang Fuqiang, Cheng Hua, et al. Difference of the two kinds of resolution DEM at different spatial scales: A caseof hilly region in Loess Plateau [J]. Journal of West China Forestry Science, 2020,49(4):54-59,67.
汤国安,赵牡丹,李天文,等.DEM提取黄土高原地面坡度的不确定性[J].地理学报,2003,58(6):824-830. Tang Guoan, Zhao Mudan, Li Tianwen, et al. Modeling slope uncertainty derived from DEMsin Loess Plateau [J].Acta Geographica Sinica, 2003,58(6):824-830.
Wang Shuyuan, Zhu Xiaoli, Zhang Wenbo, et al. Effect of different topographic data sources on soil loss estimation for a mountainouswatershed in Northern China [J]. Environmental Earth Sciences, 2016,75(20):1382.
胡云华,贺秀斌,毕景芝.直方图匹配算法进行坡度变换的精度评价[J].水土保持研究,2013,20(6):97-101. Hu Yunhua, He Xiubin, Bi Jingzhi. Assessment on the accuracy of the histogram matching algorithm for slope correction [J]. Research of Soil and Water Conservation,2013,20(6):97-101.
李发源,汤国安,贾旖旎,等.坡谱信息熵尺度效应及空间分异[J].地球信息科学,2007,9(4):13-18. Li Fayuan, Tang Guoan, Jia Yini, et al. Scale effect and spatial distribution of slope spectrum’s information entropy [J]. Journal of Geo-Information Science, 2007,9(4):13-18.
0
Views
49
下载量
0
CSCD
Publicity Resources
Related Articles
Related Author
Related Institution
京公网安备11010802024621